Претрага
792 items
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Serbian NER&Beyond: The Archaic and the Modern Intertwinned
U ovom radu predstavljamo srpski književni korpus koji se razvija pod okriljem COST Akcije „Distant Reading for European Literary History” CA16204. Koristeći ovaj korpus romana napisanih pre više od jednog veka, razvili smo i učinili javno dostupnim Sistem za prepoznavanje imenovanih entiteta (NER) obučen da prepozna 7 različitih tipova imenovanih entiteta, sa konvolucionom neuronskom mrežom (CNN), koja ima F1 rezultat od ≈91% na test skupu podataka. Ovaj model je dalje ocenjen na posebnom skupu podataka za evaluaciju. Završavamo poređenje ...... Cvetana Krstev, Ranka Stanković, Milica Ikonić Nešić Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Serbian NER&Beyond: The Archaic and the Modern Intertwinned | Branislava Šandrih Todorović, Cvetana Krstev, Ranka Stanković, Milica Ikonić Nešić | Proceedings of ...
... Belgrade Faculty of Mining and Geology ranka.stankovic@rgf.bg.ac.rs Cvetana Krstev University of Belgrade Faculty of Philology cvetana@matf.bg.ac.rs Milica Ikonić Nešić University of Belgrade Faculty of Philology milica.ikonic.nesic@fil.bg.ac.rs Abstract In this work, we present a Serbian litera- ry ...
... or completely forgotten, as judged by the number of reprints, and d) female and male authors (Frontini et al., 2020). The last version of the ELTeC (v. 1.1.0) was released in April 2021.6 It contained 14 5spaCy, https://spacy.io/ 6ELTeC (Distant Reading for European Literary Hi- language sub-collections ...Branislava Šandrih Todorović, Cvetana Krstev, Ranka Stanković, Milica Ikonić Nešić. "Serbian NER&Beyond: The Archaic and the Modern Intertwinned" in Proceedings of the Conference Recent Advances in Natural Language Processing - Deep Learning for Natural Language Processing Methods and Applications, INCOMA Ltd. Shoumen, BULGARIA (2021). https://doi.org/10.26615/978-954-452-072-4_141
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Threshold-induced correlations in the Random Field Ising Model
... ˆT i b V T i V b S i b V b S i V(S ; ) ( ; )/ , (S ; ) ( ; ), (4)b x b x x th th th 1 th hold for the duration T(i; Vth) and size ∫= ′ ′ −S i V f t dt V T i V( ; ) ( ) ( ; ) t t ith th th s e , and also for the following types of waiting times: = = = ˆ ˆ ˆ T i b V T i V b T i b V T i V ...
... =ζ ζ+ − + −D T b b V b b D T V D b S b V b b D S V( / ; , ) ( ; , ), ( ; , ) ( ; , ), (13)T x w T S x x w x Sth 1 th 1 th 1 th λ λ=ζ +D T b b V b b D T V( / ; , ) ( ; , ), (14)T x w Tint th 1 int thint int λ λ λ λ = = . ζ ζ + + D T b b V b b D T V D T b b V b b D T V ( / ; , ) ( ; , ...
... )i T( ) int th int , n T V( ; )i T( ) end th end , and n T V( ; )i T( ) ini th ini corresponding to internal waiting time Tint, and contributions Tend and Tini to the external waiting time, respectively. �ese numbers obey: = =− ˆ ˆn T b b V n T V n b S b V n S V( / ; ) ( ; ), ( ; ) ( ; ), (8)i ...Sanja Janićević, Dragutin Jovković, Lasse Laurson, Đorđe Spasojević. "Threshold-induced correlations in the Random Field Ising Model" in Scientific Reports, Springer Science and Business Media LLC (2018). https://doi.org/10.1038/s41598-018-20759-6
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Parameter determination of soil oscillation law using quotient of the relative growth increments of oscillation velocity and reduced distances at “Nepričava“ open pit mine
... operation of relation (10) we obtain: 1 21 1 2 1 ... log log ... N N N N v v vR n R R R v where we find: 1 2 1 1 1 2 ... log log ... N N N N v v v v n R R R R (11) By the replacement ...
... R1, i = 2, 3, ..., N, from the equation (9), we can take that: 1 1 2,3,..., n i i R v v i N R from where the relation is obtained: 1 1 2 1 1 2 ... ... n N N N N R v v v v R R R (10) From the relation (10), we can determine ...
... have approximately the same value (Lutovac, 2010) which will be marked (-n), meaning that: v v n R R (2) Thereby it can be considered that: 0 lim R v v n R R which means that is: 12 ...Suzana Lutovac, Sanja Bajić, Marina Ravilić, Radmila Gaćina. "Parameter determination of soil oscillation law using quotient of the relative growth increments of oscillation velocity and reduced distances at “Nepričava“ open pit mine" in Underground Mining Engineering, Belgrade : University of Belgrade, Faculty of Mining and Geology (2015). https://doi.org/10.5937/podrad1526009L
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Models of Determining the Parameters of Rock Mass Oscillation Equation with Experimental and Mass Blastings
... 1%, the oscillation velocity of the soil v will decrease (increase) by approximately n% [8]. Indeed, for h = ± R 100 = ±1%R, from (12) we obtain: v ( R ± R 100 ) ≈ v(R)∓ n· R 100 · v(R) R , v ( R ± R 100 ) ≈ v(R)∓ n· v(R) 100 , v(R ± 1%R) ≈ v(R)∓ n%·v(R). (14) 3.3. Models to Determine the ...
... applied to the function v(R) from (7), in the final growth increment, we obtain: v(R + h) ≈ v(R) + h·v′(R + θ·h), 0 < θ < 1. (11) For small absolute values h, from (11), we obtain the relation: v(R + h) ≈ v(R) + h·v′(R). (12) Having (10) in mind, relation (12) becomes: v(R + h) ≈ v(R)− n·h·v(R) R . (13) ...
... written in the form: v(R) = K-R™. (7) Then from the Equation (7) for the derivation v’(R), we obtain: o'(R) = —n-K-R-"1, (8) Minerals 2018, 8, 70 5 of 18 which may be written in the form: v′(R) = − n R ·K·R−n. (9) Having in mind Equation (7), from the Equation (9), we obtain: v′(R) = −n·v(R) R ...Suzana Lutovac, Branko Gluščević, Rade Tokalić, Jelena Majstorović, Čedomir Beljić. "Models of Determining the Parameters of Rock Mass Oscillation Equation with Experimental and Mass Blastings" in Minerals, Basel : MDPI AG, Basel, Switzerland (2018). https://doi.org/10.3390/min8020070
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Soil oscillation law parameter determination with the application of Lagrange’s theorem at “Kovilovača“ open pit
... values v(Rs), v(R1), Rs and R1 we take from the table of experimental data, so that we have: c s s Rv v 1 1 R-R v- . (12) In this manner we find a derivative v'(Rc) at point Rc, whereas Rc is given using formula (11). In practice the formula (8) is used so that the values v(Rs) and v(R1) ...
... formuli (8) vrednosti v(Rs), v(R1), Rs i R1 uzimamo iz tabele eksperimentalnih podataka, tako da imamo: c s s Rv v 1 1 R-R v- . (12) Na ovaj način nalazimo izvod v'(Rc) u tački Rc, gde je Rc dato pomoću formule (11). U praksi formulu (8) koristimo tako što vrednosti v(Rs) i v(R1) uzimamo iz ...
... i.e. n RK R n v . (5) Bearing in mind (4), equation (5) is re- duced to: R vn v (6) From (6) the following is found: v R vn (7) If the derivative v' at some point Rc could not be found then from the equation (7), n can be determined. Value of deriva- tive v' can be determined using ...Suzana Lutovac, Nebojša Vidanović, Čedomir Beljić, Zoran Gligorić. "Soil oscillation law parameter determination with the application of Lagrange’s theorem at “Kovilovača“ open pit" in Mining and Metallurgy Engineering Bor, Bor : Mining and Metallurgy Institute Bor (2015). https://doi.org/10.5937/MMEB1503053L
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Photocatalytic Activity of the V2O5 Catalyst toward Selected Pharmaceuticals and Their Mixture: Influence of the Molecular Structure on the Efficiency of the Process
Sanja J. Armaković, Aleksandra Jovanoski Kostić, Andrijana Bilić, Maria M. Savanović, Nataša Tomić, Aleksandar Kremenović, Maja Šćepanović, Mirjana Grujić-Brojčin, Jovana Ćirković, Stevan Armaković (2023)Due to the inability of conventional wastewater treatment procedures to remove organic pharmaceutical pollutants, active pharmaceutical components remain in wastewater and even reach tap water. In terms of pharmaceutical pollutants, the scientific community focuses on -blockers due to their extensive (over)usage and moderately high solubility. In this study, the photocatalytic activity of V2O5 was investigated through the degradation of nadolol (NAD), pindolol (PIN), metoprolol (MET), and their mixture under ultraviolet (UV) irradiation in water. For the preparation of V2O5, facile ...DFT analysis, metoprolol, nadolol, nanomaterial characterization, photocatalysis, pindolol, β-blocker... platelet, estimated as 25.47% for V and 74.53% for O, are close to the values of stoichiometric V5»Os. Molecules 2023, 28, 655 5of18 Spectrum 1 V A o A |A o 1 2a 3 4 5 6 7/ B 0 10 Full Scale 4432 cts Cursor:-0.124 KeV (0 cts) keV v Spectrum 2 V o V r - ——— e O 1 2 3 4 5 6 7 8 9 ...
... good crystallinity of the V>»Os phase [30—32]. A broad feature at ~1020 cm !1 may be ascribed to surface VOx species on V>Os [33]. R a m a n in te ns it y 100 200 300 400 500 600 700 800 900 1000 1100 1200 Raman shift (cm) Figure 5. Experimental Raman spectrum of V»Os catalyst (after a baseline ...
... was used to prepare V»Os powders [14,48]. For that purpose, 0.1 M ammonium metavanadate (NHaVOx) was dissolved in 80 mL of distilled water, resulting, in a pale yellow solution. To adjust the pH of the reaction solution to about 4, the diluted acetic acid (C(HaCOOH/Hx»O = 1:1 v/v) was added drop-wise ...Sanja J. Armaković, Aleksandra Jovanoski Kostić, Andrijana Bilić, Maria M. Savanović, Nataša Tomić, Aleksandar Kremenović, Maja Šćepanović, Mirjana Grujić-Brojčin, Jovana Ćirković, Stevan Armaković. "Photocatalytic Activity of the V2O5 Catalyst toward Selected Pharmaceuticals and Their Mixture: Influence of the Molecular Structure on the Efficiency of the Process" in Molecules, MDPI AG (2023). https://doi.org/10.3390/molecules28020655
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Named Entity Recognition for Distant Reading in ELTeC
Francesca Frontini, Carmen Brando, Joanna Byszuk, Ioana Galleron, Diana Santos, Ranka Stanković (2020)Akcija COST „Udaljeno čitanje za evropsku književnu istoriju“, koja je počela 2017. godine, ima među svojim glavnim ciljevima stvaranje višejezične zbirke evropskih književnih tekstova (ELTeC) otvorenog koda. U ovom radu predstavljamo rad koji je obavljen na ručnom označavanju selekcije ELTeC kolekcije za imenovane entitete, kao i na proceni postojećih alata za prepoznavanje imenovanih entiteta u pogledu njihove sposobnosti da automatski urade takve anotacije. U poslednjem paragrafu se razmatraju zajedničke tačke između ove inicijative i CLARIN-a.... R S ) , p la c e s (L O C ), e v e n ts (E V E N T ) , o rg a n is a tio n s (O R G ) (s e e T a b le 1). H o w e v e r , th is a n n o ta t io n w a s la te r s im p lif ie d to a v o id n e s te d a n n o ta tio n s a n d o v e r la p . D E M O E V E N T L O C O R G O T H E R P E ...
... lo c a tio n s in n o v e ls . 6F o r P o r tu g u e s e , tw o se ts o f n o v e l e x c e rp ts a re a v a ila b le : p o r1 c o m p ris e s c a n o n ic a l n o v e ls , in m o d e rn o r to g ra p h y , w h ile p o r2 w a s c re a te d f ro m n o v e ls w ith o ld o rto ...
... a g e s a s c o m p a ra b le a s p o s s ib le , th e n o v e ls a re s e le c te d to re p re s e n t a ) v a r io u s ty p e s o f n o v e ls a s to th e i r le n g th : sh o r t s to r ie s , e p ic n o v e ls , b ) fiv e tw e n ty -y e a r t im e p e r io d s w ith ...Francesca Frontini, Carmen Brando, Joanna Byszuk, Ioana Galleron, Diana Santos, Ranka Stanković. "Named Entity Recognition for Distant Reading in ELTeC" in CLARIN Annual Conference 2020, Oct 2020, Virtual Event, France, CLARIN (2020)
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On the distribution modulo 1 of the sum of powers of a Salem number
Dragan Stankov (2016)It is well known that the sequence of powers of a Salem number θ, modulo 1, is dense in the unit interval, but is not uniformly distributed. Generalizing a result of Dupain, we determine, explicitly, the repartition function of the sequence , where P is a polynomial with integer coefficients and θ is quartic. Also, we consider some examples to illustrate the method of determination.Algebraic integer, the house of algebraic integer, maximal modulus, reciprocal polynomial, primitive polynomial, Schinzel-Zassenhaus conjecture, Mahler measure, method of least squares, cyclotomic polynomialsDragan Stankov. "On the distribution modulo 1 of the sum of powers of a Salem number" in Comptes rendus Mathematique (2016). https://doi.org/10.1016/j.crma.2016.03.012
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Pleistocenski sisari iz jame Propas u Činiglavcima kod Pirota
Dimitrijević, V., Bogićević Katarina, Gajović, V., Vlastić Stefan. "Pleistocenski sisari iz jame Propas u Činiglavcima kod Pirota" in Zbornik radova 7. simpozijuma o zaštiti karsta, Bela Palanka, 2013. / [organizator] Akademski speleološko-alpinistički klub = Proceedings [of] 7th Symposium on Karst Protection, Beograd:Akademski speleološko-alpinistički klub (2013): 83-88
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Влияние русских иммигрантов в развитие геологии в Сербии
Banjac Nenad, Dulić Ivan (2010)Banjac Nenad, Dulić Ivan. "Влияние русских иммигрантов в развитие геологии в Сербии" in Зборник радова 15. конгреса геолога Србије са међународним учешћем, Београд, [26-29 мај] 2010. = Proceedings of the 15th Congress of Geologists of Serbia with International Participation, Belgrade [26-29 May] 2010, Belgrade:Serbian Geological Society (2010): 695-698
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An integrated study of thermal treatment effects on the microstructure and magnetic properties of Zn-ferrite nanoparticles
Antić Bratislav V., Perović Marija, Kremenović Aleksandar, Blanuša Jovan L., Spasojević Vojislav V., Vulić Predrag, Bessais Lotfi, Božin Emil S. (2013)Antić Bratislav V., Perović Marija, Kremenović Aleksandar, Blanuša Jovan L., Spasojević Vojislav V., Vulić Predrag, Bessais Lotfi, Božin Emil S.. "An integrated study of thermal treatment effects on the microstructure and magnetic properties of Zn-ferrite nanoparticles" in Journal of Physics – Condensed Matter 25 no. 8, Bristol:IOP Publ. Ltd. (2013): 1-13. https://doi.org/10.1088/0953-8984/25/8/086001
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Geonasleđe Golije i Peštera
Ljiljana V. Grujičić-Tešić (2017-09-01)Sprovedena istraživanja u ovoj studiji obuhvatila su izdvajanje, opis, evaluaciju i valorizaciju objekata geonasleđa u cilju razvoja istraživane oblasti sa stanovišta geonauka, geoturizma i geoekologije. Na izučavanom području objekti geonasleđa su evidentirani, interpretirani, vrednovani i kategorisani, dat je predlog promocije geoobjekata, i na kraju predložena dopuna inventara objekata geonasleđa Srbije.U protekle četiri godine, na kompleksu geotopa Golije i Peštera istražena su geološka svojstva stena (tip stene, starost, fosilni sadržaj, morfološke i hidrogeološke karakteristike itd.), na osnovu čega je bilo ...... RANJIVOST (R) U K U P N A V R E D N O S T ( U V O ) = (3 × N Z ) + ( 2 × D V ) + ( 2 × U V ) + (2 × R ) / 2 ,5 Je di ns tv en os t (J ) R ep re ze nt at iv no st ( R P ) K om pl ek sn os t (K ) O br az ov na v re dn os t (N O ) N ...
... ) D V = E K + K F + ( 2 × E F ) Pr ist up ač no st (P R) V id lj iv os t ( V D ) D ru gi o bj ek ti u ok tu že nj u (D R) Tu ris tič ka in fra str uk tu ra (T I) E ko no m sk i p ot en ci ja l (E P ) U V = P R + V D + ...
... Ljiljana V. Grujičić - Tešić Doktorska disertacilja GEONASLEĐE GOLIJE I PEŠTERA 85 S li k a 6 2 . S p ru d n a g re d a , S v il a n o v o , k o o rd in a te : 74 45 93 5; 4 78 96 65 , f ot o Lj .G ru jič ić - T eš ić Ljiljana V. Grujičić ...Ljiljana V. Grujičić-Tešić. "Geonasleđe Golije i Peštera" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2017-09-01)
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Hydrographic and hydrological characterization of the Vodenička and Rosomačka rivers
Vesna Ristić Vakanjac, Marina Čokorilo Ilić, Dušan Polomčić, Dragoljub Bajić, Jelena Ratković (2017)The Visočica River rises in Bulgaria, on the Berovo Mountain. Its course in Bulgaria is 16.7 km long. It enters Serbia near the village of Donji Krivodol. Up to the village of Pakleštica, or the beginning of Lake Zavoj, its right-bank tributaries are the Krivodolštica, the Vodenička, the Rosomačka and the Dojkinačka. There are no left-bank tributaries. Among the tributaries, water levels and discharges are gauged only on the Dojkinačka River. The Vodenička had also been gauged but only ...... границом и то од Бегове куле (1668 м н. в.) на исток и југоисток преко Мучибабе (1719 м н. в.), Големог гувна (1580 м н. в.), Аџијине корије (1716 м н. в.), затим преко врхова са котама 1622 м н. в., 1613 м н. в., 1609 м н. в., 1423 м н. в., до врха са котом 1368 м н. в. код Равништа, где напушта државну ...
... (955 м н. в.), Росомачког врха (1236 м н. в.), Игиног вртопа (1276 м н. в.), Чуке (1310 м н. в.), Тупанца (1602 м н. в.), а затим преко Штављака излази на државну границу између Србије и Бугарске код врха Добро јутро. Вододелница даље прати државну границу до Бегове куле (1658 м н. в.). Код врха ...
... правцем на југ одвајајући слив Росомачке реке од Воденичке и то преко врха Црнак (1592 м н. в.), затим Мешковог рида (1351 м н. в.), Сенокошке чуке (1328 м н. в.), Љиљка (1326 м н. в.), Градишта (1191 м н. в.) па све до Славиње, где је и ушће Росомачке реке у реку Височицу. Облик слива је издуженог ...Vesna Ristić Vakanjac, Marina Čokorilo Ilić, Dušan Polomčić, Dragoljub Bajić, Jelena Ratković. "Hydrographic and hydrological characterization of the Vodenička and Rosomačka rivers" in Pirotski zbornik, Pirot : Narodna biblioteka Pirot (2017). https://doi.org/10.5937/pirotzbor1742001R
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The application of ArcGIS for assessing the potential of solar energy in urban area: The case of Vranje
In order to determine the solar energy potential for a specified location, it is crucial to consider the latitude, altitude, slope, terrain morphology, atmospheric conditions, etc. Such a complex calculation and mapping of solar energy can be done using the ArcGIS geoprocessing tool, named Area Solar Radiation (ASR). By using the ASR tool, supported with the adequate input data, it is possible to calculate the maximum solar radiation energy (irradiation) for a defined area and for a specified time ...... case of Vranje Boban Pavlović, Milica Pešić-Georgiadis Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] The application of ArcGIS for assessing the potential of solar energy in urban area: The case of Vranje | Boban Pavlović, Milica Pešić-Georgiadis | 12th Int ...
... of solar energy in urban area: The case of Vranje Boban PAVLOVIĆ ! Junior researcher, Faculty of Mining and Geology, University of Belgrade Milica PEŠIĆ-GEORGIADIS Teaching assistant, Faculty of Mining and Geology, University of Belgrade ! Contact details of corresponding author Tel: +38 ...Boban Pavlović, Milica Pešić-Georgiadis. "The application of ArcGIS for assessing the potential of solar energy in urban area: The case of Vranje" in 12th International Conference on Energy and Climate Change, 9-11 October 2019, Athens - Greece, Energy Policy and Development Centre (KEPA) of the National and Kapodistrian University of Athens (2019)
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Petrofizička svojstva krečnjaka postamenta spomenika „Pobednik” na Beogradskoj tvrđavi
Dijana Trajković (2024)Spomenik „Pobednik” je podignut 1928. godine na Gornjem gradu Beogradske tvrđave. Spomenik je predstavljen bronzanom muškom figurom sa orlom u desnoj ruci i spuštenim mačem u levoj ruci i delo je vajara Ivana Meštrovića, dok je postament delo arhitekte Petra Bajalovića. Postament je u vidu dorskog stuba sa kanelurama na visokoj kubičnoj bazi i izgrađen je od krečnjaka o čijem poreklu ne postoje zvanični literaturni podaci, ali u korelaciji sa ostalim objektima Beogradske tvrđave, pretpostavlja se da je za ...... Matović, V., Gajić, V., Vasić, N., 2019. Metode ispitivanja sedimentnih stena. Univerzitet u Beogradu, Rudarsko – Geološki fakultet., str. 237- 241 Novaković, N., 2019. IDP — Idejni projekat rekonstrukcije i restauracije, Zavod za zaštitu spomenika kulture grada Beograda. Čubrilović, V. (ur.), ...
... SBIOJ 0U2O1 PODIJ 9 J O bUODI PBna(j SPJ3} 0221 PAILJ sl umfiAnjoc _ umfianjoad |___y PNMOD e{t00] *um[TAn[V | - de POBIEJS B[108} *UIm[iAn|V gpuodorl 000S0Pć 000S0Pć 00000FZ. 00000F/A . j 000S6tEZL. 000S6t2 000000S |I e = P -- = [1 .” Slika 2.4 - ...
... kasnoantičkog utvrđenja, kao i kamen sa severnih padina Kosmaja. Na to je ukazao način gradnje zapažen na Jednom delu severoistočnog bedema između kula V i VI, koji je uočen i kod manastirskih kompleksa iz XV veka na Kosmaju (Popović, 2006). U kasnijim fazama izgradnje tvrđave, nakon 1740. godine, korišćen ...Dijana Trajković. Petrofizička svojstva krečnjaka postamenta spomenika „Pobednik” na Beogradskoj tvrđavi, 2024
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Some models for determination of parameters of the soil oscillation law during blasting operations
... which will be marked ´n, meaning that: ∆v v ∆R R « ´n (7) Thereby it can be considered that: lim∆RÑ0 ∆v v ∆R R “ ´n, which means: dv v dR R “ ´n (8) Equation (8) can be written in the form: dv v “ ´n ¨ dR R , where by integration is obtained: ż dv v “ ´n ¨ ż dR R , namely: logv “ logR´n ...
... tics of the rock material, and the type of blasting, the equation of M.A. Sadovskii, where the oscillation velocity v is given in the form of the function, is most frequently used: v “ K ¨ R´n (1) where R represents reduced distance, meaning the distance from the blast site to the monitoring point ...
... soil oscillation and consequences that can affect facilities, is used. The equation of M.A. Sadovskii is given in the form: v “ K ¨ R´n “ K ¨ ˆ r 3 ? Q ˙´n (2) where we have: v—velocity of soil oscillation (m/s); K—coefficient conditioned by soil characteristics, as well as blasting conditions, where ...Suzana Lutovac, Dragan Medenica, Branko Gluščević, Rade Tokalić, Čedomir Beljić. "Some models for determination of parameters of the soil oscillation law during blasting operations" in Energies, Basel, Switzerland : MDPI (2018). https://doi.org/10.3390/en9080617
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О сопротивлении угля при резании в условиях подводной добычи
Gojković Nebojša, Čebašek Vladimir, Слободан Вуйич, Miljanović Igor, Александар Петровски, Milutinović Aleksandar (2011)Gojković Nebojša, Čebašek Vladimir, Слободан Вуйич, Miljanović Igor, Александар Петровски, Milutinović Aleksandar. "О сопротивлении угля при резании в условиях подводной добычи" in Всероссийская научная конференция „Геодинамика и напряженное состояние недр земли“, посвящена 80-летию академика М. В. Курлени, 3-6.10.2011 - no. -, Новосибирск, Россия:Институт горного дела Новосибирского научного центра Сибирского отделения Российской академии наук, Новосибирск (2011): 191-195. https://doi.org/-
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Regionalno-geološke karakteristike miocenskih sedimenata na prostoru severnog Banata
Dejan N. Radivojević (2014-12-30)Predmet doktorske disertacije predstavljalo je rešavanje strukturno‐stratigrafskihodnosa miocenskih sedimenata na prostoru severnog Banata. U cilju regionalnogsagledavanja, korišćeni su svi raspoloživi geofizički i geološki podaci sa širegistražnog područja, odnosno iz celog Panonskog basena i susednog orogena. Osimklasičnih metoda primenjene su i savremene metode seizmostratigrafije,tektonostratigrafije i riftne sekvencione stratigrafije. Primenjene metode omogućilesu izradu modela progradacije ivice šelfa za ceo Panonski basen, modela uzajamnihveza između basena i geodinamičkog modela jugoistočnog oboda basena.Jezero Panon je većim delom zapunjeno prilivom sedimenata paleo‐Dunavom saseverozapada, odnosno ...Centralni Paratetis, Panonski basen, miocen, jezero Panon,seizmostratigrafija, sekvenciona stratigrafija, paleogeografija, geodinamika... (Austroalpine, Eastern Alps), Acta Geol. Hungarica, v. 48/4, p. 371–394. Lešić, V., E. Marton, and V. Cvetkov, 2007, Paleomagnetic detection of Tertiary rotations in the Southern Pannonian Basin (Fruška Gora), Geol. Carpathica, v. 58(2), p. 185–193. Lister, G. S., and G. A. Davis ...
... Geophysical Transactions, v. 31, p. 55–74. Bérczi, I., V. Dank, S. Gajdos, S. Pap, I. Révész, K. Szentgyörgyi, and L. Völgyi, 1987, Ablagerungen der Kunság‐Stufe (Pannonien s. str.) auf der Grossen Ungarischen Tiefebene, Annals of the Hungarian Geological Institute, v. 69, p. 179–211. Bérczi ...
... Precambrian and Neogene, Episodes, v. 27, p. 83–100. Lučić, D., B. Saftić, K. Krizmanić, E. Prelogović, V. Britvić, I. Mesić, and J. Tadej, 2001, The Neogene evolution and hydrocarbon potential of the Pannonian Basin in Croatia, Mar. Petrol. Geol., v. 18, p. 133–147. Magoon, L., and ...Dejan N. Radivojević. "Regionalno-geološke karakteristike miocenskih sedimenata na prostoru severnog Banata" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2014-12-30)
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Zbirka rešenih zadataka iz termodinamike
Marija Živković, Aleksandar Madžarević (2023)... REŠENJE: Rad u p-V dijagramu je predstavljen površinom ispod promene stanja. U ovom slučaju rad je jednak površini pravouglog trapeza, kako je prikazano na slici: p, kPa p 1 =1000kPa p 2 =200kPa V 1 =0,05 m3 V 2 =0,2 m3 V, m3 1 2 Skica uz zadatak 38 Rad u p-V dijagramu je predstavljen ...
... pa je razmatrani proces izohorski. Zapremina u početnom stanju procesa jednaka je zapremini u kraj- njem stanju procesa: v 1 = v 2 Zapremina suda je poznata i iznosi: V = 23 l = 23 ∙ 10-3 m3 Za određivanje mase vlažne vodene pare potrebno je da se odredi stepen suvoće za neku od tačaka procesa ...
... temperatura vode ista u celom bazenu. REŠENJE: Posmatrani proces kretanja vazdušnog mehura sa dna na površinu bazena je izoterm- ski:1 = 2 = V 2 V 1 z Skica uz zadatak 1 Jednačina stanja idealnog gasa u mehuru za stanje 1 je:1 1 = Pritisak vazduha u mehuru u stanju 1 je:1 = + z gde ...Marija Živković, Aleksandar Madžarević. Zbirka rešenih zadataka iz termodinamike, Beograd : Univerzitet u Beogradu, Rudarsko-geološki fakultet, 2023
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Gate Road Support Deformation Forecasting Based on Multivariate Singular Spectrum Analysis and Fuzzy Time Series
Luka Crnogorac, Rade Tokalić, Zoran Gligorić, Aleksandar Milutinović, Suzana Lutovac, Aleksandar Ganić (2021)Underground mining engineers and planners in our country are faced with extremely difficult working conditions and a continuous shortage of money. Production disruptions are frequent and can sometimes last more than a week. During this time, gate road support is additionally exposed to rock stress and the result is its progressive deformation and the loss of functionality of gate roads. In such an environment, it is necessary to develop a low-cost methodology to maintain a gate road support system. ...deformacije podgrade, lasersko skeniranje, višekanalna singularna spektralna analiza, prognoza, klasterisanje fuzzy vremenskih serija... be expressed by the time-dependent position vectors as follows: → V(t) = [→ v ij ] M×N = → v 11 → v 12 → v 13 · · · → v 1N → v 21 → v 22 → v 23 · · · → v 2N ... ... ... . . . ... → v M1 → v M2 → v M3 · · · → v MN , (3) The position of each marker is represented by each ...
... = 0, 1, . . . , 5 and t = 6, 7, 8 is represented in Table 16. Table 16. Displacement intensity vector ∆V. Marker ∆v(t = 0) ∆v(t = 1) ∆v(t = 2) ∆v(t = 3) ∆v(t = 4) ∆v(t = 5) ∆v(t = 6) ∆v(t = 7) ∆v(t = 8) 1 0.000 0.011 0.014 0.014 0.016 0.013 0.015 0.013 0.012 2 0.000 0.019 0.016 0.018 0.018 0.014 0 ...
... variable. It can be defined as a triplet (a, b, c). The corresponding membership function is defined as [24]: µA(∆v) = 0, ∆v < a ∆v−a b−a , a ≤ ∆v ≤ b c−∆v c−b , b ≤ ∆v ≤ c 0, ∆v > c , (21) Step 2: determine a fuzzy observation of displacement. Triangular fuzzy number O(t) =(a(t), b(t), ...Luka Crnogorac, Rade Tokalić, Zoran Gligorić, Aleksandar Milutinović, Suzana Lutovac, Aleksandar Ganić. "Gate Road Support Deformation Forecasting Based on Multivariate Singular Spectrum Analysis and Fuzzy Time Series" in Energies, MDPI (2021). https://doi.org/https://doi.org/10.3390/en14123710